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Earthquake nucleation and fault slip complexity in the lower crust of central Alaska

Earthquake nucleation and fault slip complexity in the lower crust of central Alaska

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_hal_primary_oai_HAL_hal_02019296v1

Earthquake nucleation and fault slip complexity in the lower crust of central Alaska

About this item

Full title

Earthquake nucleation and fault slip complexity in the lower crust of central Alaska

Publisher

London: Nature Publishing Group UK

Journal title

Nature geoscience, 2018-07, Vol.11 (7), p.536-541

Language

English

Formats

Publication information

Publisher

London: Nature Publishing Group UK

More information

Scope and Contents

Contents

Earthquakes start under conditions that are largely unknown. In laboratory analogue experiments and continuum models, earthquakes transition from slow-slipping, growing nucleation to fast-slipping rupture. In nature, earthquakes generally start abruptly, with no evidence for a nucleation process. Here we report evidence from a strike-slip fault zon...

Alternative Titles

Full title

Earthquake nucleation and fault slip complexity in the lower crust of central Alaska

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_hal_primary_oai_HAL_hal_02019296v1

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_hal_primary_oai_HAL_hal_02019296v1

Other Identifiers

ISSN

1752-0894

E-ISSN

1752-0908

DOI

10.1038/s41561-018-0144-2

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